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Physical Process

Fluvial Erosion

Geomorphology

The wearing away of rock and sediment by moving river and stream water, the dominant process carving valleys, canyons and channel networks across the world's land surface. It operates through hydraulic action, abrasion by transported sediment, and the dissolution of soluble rock, with its rate governed chiefly by water velocity and the sediment load a channel carries.

Facts
Process Type
Fluvial 1
Fluvial Erosion
Filter Results5 entries
Connections

Caused By

Causes

Source Bank Erosion (Wikipedia)
Source Rill Erosion (Wikipedia)

Shaped

Colca Canyon was carved by the Colca River.

Source Colca Canyon (Wikipedia)
Sources
1. Erosion (Wikipedia)
WikipediaWikipedia: Erosion, Rivers and streams section
Quote, Wikipedia: Erosion, Rivers and streams section
Valley or stream erosion occurs with continued water flow along a linear feature. The erosion is both downward, deepening the valley, and headward, extending the valley into the hillside, creating head cuts and steep banks.
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Rill Erosion (Wikipedia)
Wikimedia FoundationCauses: Rill ErosionView the Source
Bank Erosion (Wikipedia)
Wikimedia FoundationCauses: Bank ErosionView the Source
Colca Canyon (Wikipedia)
Wikimedia FoundationShaped: Colca Canyon, Lead section
Quote, Shaped: Colca Canyon, Lead section
The Colca Canyon is a canyon of the Colca River in southern Peru.
View the Source
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